Sichuan section mainstem (SSM) in the upper Yangtze River (UYR) plays a crucial role in protecting the aquatic environment of the UYR and ensuring a safe water supply to the Three Gorges Reservoir. The impoundments of cascade reservoirs on the lower Jinsha River have significantly influenced sediment regime and phosphorus (P) transport in the SSM. This effect on water quality and safety remains poorly understood. In this study, the spatiotemporal variations of P fraction and distribution in the SSM from 2010 to 2020 were measured. The results showed that critical changes were observed in the SSM after the impoundment in 2012, which were as follows: (1) in the outflow of the SSM, dissolved phosphorus (DP) flux increased from 0.950×104t to 1.153×104t and the proportion of DP in the total phosphorus (TP) increased by 227.4%. Jinsha River, Min River, and DP release from internal P, bore responsibilities of 24.6%, 38.9%, and 21.3% for the DP growth, respectively. (2) Min River replaced Jinsha River as the dominant P supplier. (3) Concentrations of TP, particle phosphorus (PP), coarse particle P (CPP), and fine particle P (FPP) were positively related with SS concentration (R2>84%). Proportions of PP and DP in TP showed substantial logarithmic increase and decrease over SS concentration (R2>95%), respectively. The proportion of FPP in PP was elevated by 32.5%, whereas that of FPP in TP remained stable in both the SSM and its tributaries from 2010 to 2020 and had a relatively close value (35.9 to 39.9%). The important phenomenon, not reported in previous studies, will need detailed exploration to reveal the reasons and scientific significances in future work. These findings elucidated the transformation of P species along the SSM, providing a comprehensive understanding of FPP and CPP in preventing and controlling P pollution in the SSM.
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